Compact Thescelosaurus Year Nine

October and National Fossil Day have rolled around again (check out the fall 2024 Park Paleontology News, too!), so it's time to take a look at the previous year's changes to The Compact Thescelosaurus and welcome some new content. First, the new stuff: I'm sure you'll be shocked to find out I've followed up Triassic pseudosuchians with... Jurassic pseudosuchians. I'm rearranging the pseudosuchian content a bit, to have the non-crocodylomorphs on one sheet and the crocodylomorphs on another. This was done to forestall the deployment of an unwieldy number of "subdivision" columns. Provided I get far enough along, something similar might have to happen with the new sheet around Crocodylia or so. Anyway, the main takeaways I got out of Jurassic pseudosuchians are 1) there's been a lot of work on thalattosuchians over the past couple of decades, and 2) I've discovered I'm not very fond of thalattosuchians and certainly don't mind that they conk out midway through the Cretaceous.

Hey, it's the Science Museum "Goniopholis" again! (Most Jurassic pseudosuchians are thalattosuchians, but North America is largely bereft of the darlings, so we make do with crocs like these.)

Rockford, Part 2: Fossils (exclusive of brachiopods)

Before we get into the festivities, I've recently written an article for the online magazine Agate, about identifying common Paleozoic fossils of Minnesota. It's a compact summary that covers the most abundant groups, so if you're looking for something like that, go have a look!

In our previous post we had a look at the geology of the Fossil & Prairie Park Preserve of Floyd County, Iowa, also known as the Rockford site. For this post I'm going to briefly detail the fossils I collected, with the exception of the brachiopods, which will get a post of their own. For most of the non-brachiopods, I didn't get too far into the weeds on taxonomy, because many of the groups don't lend themselves to simple eye-checks for genera and species. Horn corals and bryozoans, for example, usually require thin sections, and crinoid columnals are generally only diagnostic of the presence of crinoids. I did, though, have recourse to Fenton and Fenton (1924) and other peoples' identifications to get some ideas.

Rockford, Part 1: The Site

A few weeks I was able to join a Geological Society of Minnesota field trip to the Fossil & Prairie Park Preserve of Floyd County, Iowa, which to some of you may be more familiar as the Rockford site. We ended up having a practically ideal day: pleasant temperatures, clear skies, dry conditions, and a light breeze. If you have an itch to collect fossils (an itch that's becoming difficult to legally scratch in Minnesota these days), I highly recommend a visit.

A view into the old quarry directly south of the parking area.

Your Friends The Titanosaurs: Qunkasaura pintiquiniestra

2024 has been a great year for new titanosaurs, as we are now on the fifth to be announced and we're still more than three months from the end of the year. For a change of pace, this time we're heading to Europe. Qunkasaura pintiquiniestra, the first new European titanosaur in more than two and a half years, hails from the Lo Hueco site in Spain.

Fona herzogae

This whole thing started from a website called Thescelosaurus!, so unsurprisingly I'm particularly interested when an old-fashioned "hypsil" metaphorically crosses my desk. Our (belated) guest today is the new genus and species Fona herzogae. Before we get into the meat of the post, I would also like to throw a kind word to the iguanodontian Comptonatus chasei Lockwood et al. (2024), published online the same day. (Yes, it *did* make me think of Camptonotus, which would have been Camptosaurus had somebody not pinned it to a cricket first.)

An unexpected mammoth

While visiting Wisconsin's Interstate Park over the weekend (happy 80th birthday, Smokey Bear!), I was surprised to come across another resident of the Cottage Grove area at the Ice Age Center:

According to the display, this mammoth tooth was discovered on Grey Cloud Island on July 9, 1987, by Arnold Sanford of Frederic, Wisconsin. This is the kind of thing that makes me wish we had an update to Stauffer "1945". (Even if I have to do it myself.) There must be plenty of other post-WWII finds scattered across Minnesota that are only known locally. When I was a little kid, my mother told me that part of a mammoth tooth had been found in Red Wing by a Boy Scout; I've never been able to find anything about it, but it certainly wouldn't surprise me!

Incidentally, the Ice Age Center also has other fossils and cast fossils of Ice Age mammals from the area. (Interstate Park is the western terminus of the Ice Age National Scenic Trail and one of the components of Ice Age National Scientific Reserve.) The most significant are bison bones and a cast skull from the park's bison bonebed, discovered in 1936 during CCC work. The bonebed is in my hopper of topics; until then, here are the specimens on display.

References

Stauffer, C. R. “1945” [at least 1948 based on dates in the article]. Some Pleistocene mammalian inhabitants of Minnesota. Minnesota Academy of Science Proceedings 13:20–43.

Silver Creek Cliff geology

For obvious reasons, this blog has featured plenty of sedimentary rocks, but hardly a crystalline rock (one notable exception being World of Stone, which also allowed me to title a post after an obscure George Harrison song; no particular reason although in hindsight I might have been feeling down at the time). I just got back from a trip to Duluth and the North Shore and discovered my phone had secretly and unexpectedly created this grand panorama of a spectacular roadcut, so I thought I'd mix up the usual topics:

Definitely worth the click to embiggen

This location is the north end of the Highway 61 tunnel at Silver Creek Cliff, where there is a fun roadside pullout with information about the construction of the tunnel (and the former route of Highway 61, which went where the walking path is now and looks like it would have been extremely narrow). What we're looking at is a sequence of events in the old Midcontinent Rift, 1.1 billion years ago. There is an annotated photo showing part of the roadcut here, but most of the different things are easy to spot without too much guidance. On the right, the somewhat pinkish rocks beginning above the road are flows of andesite, a type of volcanic igneous rock. The andesite is cut off by a stark, irregular contact with a dark blue-gray rock; the contact begins near the blue minivan and rises going to the right. The darker rock is diabase, an igneous rock that intrudes into existing rock underground and has a similar composition to basalt. The diabase makes up most of the roadcut, but you may notice a weird "scar" running through it. It begins, from the perspective of the flat image, just right of the right-most metal structure on our side of the road (the one right of the street light pole) and rises to the right until it is lost under vegetation. This "scar" is laced with light-colored rocks. It represents diabase that has been altered by faulting, with new minerals forming in the fault gouge. Thus, the sequence of events is: 1) eruption of andesite; 2) intrusion by diabase; 3) faulting and mineralization within the diabase.

The key part of the panorama, showing the andesite, diabase, and fault.